Final answer:
Potassium-Argon Radiocarbon Dating is a method used to determine the age of rocks and minerals based on the decay of radioactive isotopes.
Step-by-step explanation:
Potassium-Argon Radiocarbon Dating, recognized as an absolute dating technique, serves to ascertain the age of rocks and minerals through the analysis of radioactive isotope decay.
This method focuses on the ratio of Argon-40 (Ar-40) to Potassium-40 (K-40) within a rock specimen.
The process involves measuring the quantity of Ar-40 released upon crushing the rock.
Scientists leverage this data to determine the rock's age, employing the established half-life of K-40, which spans 1.25 billion years.
The efficacy of Potassium-Argon Radiocarbon Dating lies in its reliance on the predictable decay of isotopes, offering researchers a valuable tool to unravel the chronological mysteries of geological formations.
It gain insights into Earth's historical timeline through the systematic assessment of radioactive decay in rock samples.